Analysis of Thermal Behaviour in the Active Layer of Degrading Mountain Permafrost
Mountain permafrost is highly susceptible to the effects of climate warming, because its thermal regime is close to 0 °C. This can be evidenced by the acceleration of average annual creep rates of several rock glaciers in the Swiss Alps, whereby some exhibit even more extreme signs of degradation. M...
Published in: | Permafrost and Periglacial Processes |
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Main Authors: | , , , , |
Format: | Article in Journal/Newspaper |
Language: | unknown |
Subjects: | |
Online Access: | https://doi.org/10.1002/ppp.1827 |